Antipode Calculator

Find the antipodal point (opposite side of Earth) for any coordinates. Visualize the exact location diametrically opposite to your position on the globe.

Negative for South (-90 to 90)
°
Negative for West (-180 to 180)
°
Your Location
40.7128° N, 74.0060° W
Hemisphere: Northern & Western
Antipodal Point
40.7128° S, 105.9940° E
Hemisphere: Southern & Eastern
Through Earth Distance
12,742 km
7,918 miles through Earth's center
Surface Distance
20,015 km
Maximum great-circle distance (half circumference)
Approx. Time Zone Diff
~12 hours
UTC-5 → UTC+7
Opposite Season
Southern Hemisphere
Your antipode experiences the opposite season

Visual Coordinate Shift

Latitude Flip
90°N90°S
Longitude Shift (±180°)
180°W180°E

World Cities Antipode Reference

CityCoordinatesAntipodeAntipode Region
New York, USA40.71°, -74.01°-40.71°, 105.99°Southern Ocean/Antarctica area
London, UK51.51°, -0.13°-51.51°, 179.87°Southern Ocean/Antarctica area
Tokyo, Japan35.68°, 139.65°-35.68°, -40.35°Southern Ocean/Antarctica area
Sydney, Australia-33.87°, 151.21°33.87°, -28.79°Northern hemisphere
Madrid, Spain40.42°, -3.70°-40.42°, 176.30°Southern Ocean/Antarctica area
Wellington, NZ-41.29°, 174.78°41.29°, -5.22°Northern hemisphere
Rio de Janeiro-22.91°, -43.17°22.91°, 136.83°Indian/Pacific Ocean
Beijing, China39.90°, 116.41°-39.90°, -63.59°Southern Ocean/Antarctica area
Mumbai, India19.08°, 72.88°-19.08°, -107.12°Pacific Ocean
Nairobi, Kenya-1.29°, 36.82°1.29°, -143.18°Atlantic/Africa region
Planning notes, formulas, and examples

About the Antipode Calculator

Ever wondered what's on the exact opposite side of the Earth from where you stand? The antipodal point — or antipode — is the location diametrically opposite any point on Earth's surface. If you could drill a straight line through the center of the planet, you'd emerge at your antipode. This calculator computes that point for any set of geographic coordinates.

Contrary to popular belief, most land-based antipodes don't correspond to other land masses. In fact, only about 4% of Earth's land surface has a land antipode. If you're in North America, your antipode is almost certainly in the Indian Ocean. Europeans find their antipodes near New Zealand and in the Pacific. This calculator shows you exactly where your opposite point falls and provides details about the nearest landmass.

Our Antipode Calculator is useful for geography education, travel planning curiosity, satellite communication analysis, and understanding Earth's geometry. Enter any latitude and longitude — or choose from popular city presets — and discover what lies on the other side of the world. The tool also calculates the great-circle distance through Earth's center and shows the time zone difference.

When This Page Helps

Satisfy geographic curiosity, teach Earth geometry concepts, or plan around-the-world routes. This calculator shows the opposite side of the globe for any location. This calculator handles the repetitive math so you can compare scenarios, verify assumptions, and focus on the decision the result supports.

How to Use the Inputs

  1. Enter latitude in decimal degrees (-90 to 90, negative for South).
  2. Enter longitude in decimal degrees (-180 to 180, negative for West).
  3. Or select a preset city to auto-fill coordinates.
  4. View the antipodal coordinates, nearest landmark, and distance through Earth's center.
  5. Check the time zone difference and hemisphere details.
  6. Compare multiple locations using the reference table.
Formula used
Antipodal Latitude = -latitude Antipodal Longitude = longitude + 180° (if ≤ 0°) or longitude - 180° (if > 0°) Distance through Earth = 2 × Earth's radius ≈ 12,742 km Great Circle Surface Distance = π × Earth's radius ≈ 20,015 km

Example Calculation

Result: -40.7128°, 105.9940°

The antipode of New York City (40.7128°N, 74.0060°W) is at 40.7128°S, 105.9940°E, which is in the Indian Ocean southwest of Australia.

Tips & Best Practices

  • Use negative latitude for Southern hemisphere and negative longitude for Western hemisphere.
  • Google Maps shows coordinates when you right-click any location.
  • Most US antipodes land in the Indian Ocean — try it with your hometown!
  • Madrid and Wellington, NZ are the closest major-city antipodal pair.
  • The antipode of the North Pole is the South Pole, and vice versa.
  • Antipodal points always have opposite seasons (summer vs winter).

The Science of Antipodal Points

The concept of antipodal points goes beyond simple geography. In mathematics, antipodal points are fundamental to topology and the study of spheres. The Borsuk-Ulam theorem states that for any continuous function from a sphere to the plane, there exists at least one pair of antipodal points that map to the same value — meaning at any given moment, there are two opposite points on Earth with exactly the same temperature and barometric pressure.

Computing an antipode is mathematically straightforward: negate the latitude and add or subtract 180° from the longitude. However, because Earth is an oblate spheroid rather than a perfect sphere, the actual "through the center" path would be slightly different from the calculated surface antipode. For practical purposes, the spherical approximation is more than sufficient.

Famous Antipodal Pairs

The most notable near-antipodal city pair is Madrid, Spain and Wellington, New Zealand, which are remarkably close to being exact opposites. Parts of northern Spain are almost perfectly antipodal to New Zealand's South Island. In South America, the southern tip of Argentina is antipodal to parts of Mongolia and Russia. Hawaii's antipode falls in Botswana, Africa — one of the few cases where a US location has a land-based antipode.

Some interesting geographic antipodal facts: the entire continent of Antarctica is approximately antipodal to the Arctic Ocean. The Mariana Trench in the Pacific, the deepest point on Earth, has its antipode near the Kalahari Desert in Africa. Mount Everest's antipode is in the Pacific Ocean near Easter Island.

Practical Applications

Beyond curiosity, antipodal calculations have real applications. In telecommunications, signals sent through Earth's crust (for theoretical point-to-point tunneling) or around the globe (for submarine cables and satellite routing) need to account for maximum distance calculations. Seismologists study how seismic waves from earthquakes focus at the antipodal point — after a major earthquake, sensitive instruments at the antipode can detect focused energy. In amateur radio, "long path" propagation around the back of the globe to reach near-antipodal stations is a well-known technique.

Sources & Methodology

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Frequently Asked Questions

  • An antipode (or antipodal point) is the point on Earth's surface that is diametrically opposite to a given location. It's. Use antipode coordinates as a directional check, then verify with a geolocation source. where you'd end up if you tunneled straight through the center of the Earth.